Rock Identifier
Tumbled black obsidian (Volcanic glass; rhyolitic obsidian, primarily SiO₂) — igneous
igneous

Tumbled black obsidian

Volcanic glass; rhyolitic obsidian, primarily SiO₂

AI-generated identification · may be incorrect

Hardness about 5–5.5 Mohs; black to dark brown, vitreous luster, amorphous glassy structure, no cleavage, conchoidal fracture, specific gravity roughly 2.35–2.60. The smooth surface indicates tumbling or polishing.

Identified More igneous
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Physical properties

Hardness about 5–5.5 Mohs; black to dark brown, vitreous luster, amorphous glassy structure, no cleavage, conchoidal fracture, specific gravity roughly 2.35–2.60. The smooth surface indicates tumbling or polishing.

Formation & geological history

Forms when silica-rich lava cools so rapidly that crystals cannot grow, usually at volcanic flows and domes during the Quaternary and older periods. The specimen appears human-processed rather than naturally fractured.

Uses & applications

Used for ornamental objects, cabochons, beads, tools, and historically razor-sharp blades; not generally used as structural stone. Jewelry-grade examples are collected for their glassy appearance.

Geological facts

Obsidian can produce exceptionally sharp edges and was used by prehistoric cultures for knives and arrowheads. Flow bands, snowflake patterns, or sheen varieties may occur, but none is clearly visible here.

Field identification & locations

Identify by its uniformly glassy black appearance, conchoidal fracture, lack of visible grains, and inability to scratch glass reliably despite its hardness. Common sources include Mexico, the western United States, Armenia, Iceland, and Japan.